@article{oai:kanazawa-u.repo.nii.ac.jp:00011062,
 author = {久田, 健一郎 and 荒井, 章司 and Hisada, Ken-ichiro and Arai, Shoji and Lee, Yong Il},
 issue = {3},
 journal = {Island Arc},
 month = {Sep},
 note = {In Japan and Korea, some Lower Cretaceous terrigenous clastic rocks yield detrital chromian spinels. These chromian spinels are divided into two groups: low-Ti and high-Ti. The Sanchu Group and the Yuno Formation in Japan have both groups, whereas the Nagashiba Formation in Japan and the Jinju Formation in Korea have only the low-Ti spinels. High-Ti spinels are thought to have originated in intraplate-type basalt. Low-Ti spinels (higher than 0.6 Cr) were probably derived from peridotites, which are highly correlated with an arc setting derivation and possibly with a forearc setting derivation. Low-Ti spinels are seen in the Sanchu Group, the Nagashiba Formation and the Jinju Formation. Low-Ti spinels from the Yuno Formation are characterized by low Cr (less than 0.6) and these chromian spinels appear to have been derived from oceanic mantle-type peridotite, including backarc. According to maps reconstructing the pre-Sea of Japan configuration of the Japanese Islands and the Korean Peninsula, the Korean Cretaceous basin was comparatively close to the Southwest Japan depositional basins. It is possible that these Lower Cretaceous systems were sediments mainly in the forearc and partly in the backarc regions. The peridotite might have infiltrated along major tectonic zones such as the Kurosegawa Tectonic Zone (=serpentinite melange zone) in which left lateral movement prevailed during the Early Cretaceous., 金沢大学理工研究域自然システム学系},
 pages = {336--348},
 title = {Tectonic implication of Lower Cretaceous chromian spinel-bearing sandstones in Japan and Korea},
 volume = {8},
 year = {1999}
}